GSA Annual Meeting in Seattle, Washington, USA - 2017

Paper No. 283-5
Presentation Time: 9:00 AM-6:30 PM

PROVENANCE CONTROLS ON THE GEOCHEMISTRY AND RADIOGENIC ISOTOPIC COMPOSITION OF PLEISTOCENE TILLS IN MINNESOTA USA


WITTKOP, Chad1, BARTLEY, Julie K.2, KRUEGER, Russell2, KNAEBLE, Alan R.3, BOUVIER, Audrey4, GEORG, R.Bastian5, ST. CLAIR, Katherine6 and PIPER, Christian1, (1)Department of Chemistry and Geology, Minnesota State University, Ford Hall 241, Mankato, MN 56001, (2)Geology Department, Gustavus Adolphus College, 800 W. College Ave, St. Peter, MN 56082, (3)Minnesota Geological Survey, University of Minnesota, 2642 University Avenue West, St. Paul, MN 55114, (4)Department of Earth Sciences, University of Western Ontario, London, ON N6A 5B7, Canada, (5)Water Quality Center, Trent University, Peterborough, ON K9J7B8, Canada, (6)Department of Mathematics and Statistics, Carleton College, Northfield, MN 55057, chad.wittkop@mnsu.edu

In Minnesota, Pleistocene tills from four major source regions—Riding Mountain (northwest), Winnipeg (north/northwest), Rainy (north/northeast), and Superior (northeast)—are traditionally differentiated primarily on the basis of matrix color and clast composition. Here we report on an investigation of glacial sediment provenance using a combination of geochemical approaches, including bulk sediment X-ray fluorescence (XRF), multi-element ICP-MS analysis, and Sr and Nd isotopic composition. We analyzed a series of carbonate-rich tills taken by rotasonic core from Renville County MN, as well as a series of reference till samples representing each of the major source regions described above. Glaciolacustrine samples were also examined from key localities. We conducted parallel analyses of <2-mm and <63-µm size fractions, and performed XRF and bulk X-ray diffraction (XRD) on samples before and after carbonate removal. Isotopic and ICP-MS analyses were conducted on carbonate-free samples. Principal component and discriminant function statistical analyses highlighted differences in elemental geochemistry among regionally recognized Pleistocene lithostratigraphic units, but statistical analysis did not show a dramatic difference between size fractions, suggesting that use of either fraction is justifiable. Radiogenic isotopic compositions of the fine (<63 µm) fraction show distinctive signatures consistent with bedrock source regions, and down-core trends in Sr- and Nd-isotopic composition show coherent variation relative to other provenance signatures including trace element ratios (e.g. Zr/Sc) and the chemical index of alteration. Analyzed lake sediment samples are consistent with Nd-isotopic compositions of tills from the same provenance, but trace element and Sr-isotopic signatures show evidence of alteration by processes that may include sedimentary transport or weathering. The rare-earth element compositions of glacial tills show very little relationship with provenance. Overall, our results demonstrate that a multi-element approach to Pleistocene till geochemistry is capable of providing insight into sediment provenance as well as process.